2,194 research outputs found
Hyperbolic systems of conservation laws in one space dimension
Aim of this paper is to review some basic ideas and recent developments in
the theory of strictly hyperbolic systems of conservation laws in one space
dimension. The main focus will be on the uniqueness and stability of entropy
weak solutions and on the convergence of vanishing viscosity approximations
One Dimensional Hyperbolic Conservation Laws: Past and Future
Aim of these notes is provide a brief review of the current well-posedness
theory for hyperbolic systems of conservation laws in one space dimension, also
pointing out open problems and possible research directions. They supplement
the slides of the short course given by the author in Erice, May 2023,
available at: sites.google.com/view/erice23/speakers-and-slides.Comment: 38 pages, 25 figure
The convergence of spectral methods for nonlinear conservation laws
The convergence of the Fourier method for scalar nonlinear conservation laws which exhibit spontaneous shock discontinuities is discussed. Numerical tests indicate that the convergence may (and in fact in some cases must) fail, with or without post-processing of the numerical solution. Instead, a new kind of spectrally accurate vanishing viscosity is introduced to augment the Fourier approximation of such nonlinear conservation laws. Using compensated compactness arguments, it is shown that this spectral viscosity prevents oscillations, and convergence to the unique entropy solution follows
On the convergence rate of finite difference methods for degenerate convection-diffusion equations in several space dimensions
We analyze upwind difference methods for strongly degenerate
convection-diffusion equations in several spatial dimensions. We prove that the
local -error between the exact and numerical solutions is
, where is the spatial dimension and
is the grid size. The error estimate is robust with respect to
vanishing diffusion effects. The proof makes effective use of specific kinetic
formulations of the difference method and the convection-diffusion equation
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